地理科学 ›› 2015, Vol. 35 ›› Issue (7): 898-904.doi: 10.13249/j.cnki.sgs.2015.07.898
收稿日期:
2014-02-28
修回日期:
2014-05-04
出版日期:
2015-07-20
发布日期:
2015-07-20
作者简介:
作者简介:孙 禹(1987-),男,吉林省长春市人,博士研究生,主要从事干旱区地貌与环境研究。E-mail:
基金资助:
Yu SUN1(), Hui-shi DU2, Mei-ping LIU1, HA-Si1(
)
Received:
2014-02-28
Revised:
2014-05-04
Online:
2015-07-20
Published:
2015-07-20
摘要:
风蚀坑是沙质海岸、湖岸及干旱、半干旱区沙质草原地区受风蚀作用形成的洼地。受风蚀坑地形的影响,坑内气流的风速、风向发生了变化,通过输沙过程的局部差异改变了风蚀坑的蚀积格局,并对风蚀坑形态进行改造。而形态的变化又反作用于近地表气流,由此产生风蚀坑形态-动力学的响应与反馈。总结并扼要评述国内外近年来风蚀坑形态-动力学及其发育演化方面的研究进展,分析现有研究的不足,以期对今后此类研究提供借鉴。
中图分类号:
孙禹, 杜会石, 刘美萍, 哈斯. 风蚀坑形态-动力学研究进展[J]. 地理科学, 2015, 35(7): 898-904.
Yu SUN, Hui-shi DU, Mei-ping LIU, HA-Si. A Review on Morphodynamic Processes of Blowouts[J]. SCIENTIA GEOGRAPHICA SINICA, 2015, 35(7): 898-904.
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